. Bulletin of the Department of Geology. Geology. A. Exposure of fine ashy and shaly tuff member of Rosamond Series in the south limb of syncline, showing characteristic weathering of the unconsolidated beds. At the right with a fault contact are strata of the basal breccia member. On the left in nor- mal succession are the basal beds of the resistant breccia member. The capping is of later B. Fossiliferous tuff member of the Rosamond Series exposed in the trough of the Barstow syncline, near the west end of the exposure1. The badlands are characteristic of the less consolidated por
. Bulletin of the Department of Geology. Geology. A. Exposure of fine ashy and shaly tuff member of Rosamond Series in the south limb of syncline, showing characteristic weathering of the unconsolidated beds. At the right with a fault contact are strata of the basal breccia member. On the left in nor- mal succession are the basal beds of the resistant breccia member. The capping is of later B. Fossiliferous tuff member of the Rosamond Series exposed in the trough of the Barstow syncline, near the west end of the exposure1. The badlands are characteristic of the less consolidated portion of the series. Through the middle in the middle dis- tance runs the indurated basal layer of (he later alluvium, which here dips 2° to the Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original University of California, Berkeley. Dept. of Geology. Berkeley : The University Press
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Keywords: ., bookcentury1900, bookdecade1900, booksubjectgeology, bookyear1902
